On the equivalence of the "Niblett" and "Bostick" transformations in the magnetotelluric method

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A.G. Jones


In the 1D interpretation of magnetotelluric data, it is often useful to discover a reasonable first-approximation to the true conductivity-depth distribution beneath the recording location. This may be undertaken in the field, in order to ascertain if the station spacing is satisfactory or whether a greater station density of coverage is required, or at the base laboratory, as a prelude to a more sophisticated 1D inversion of the data.

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Jones, A. (1983). On the equivalence of the "Niblett" and "Bostick" transformations in the magnetotelluric method. Journal of Geophysics, 53(1), 72-73. Retrieved from https://journal.geophysicsjournal.com/JofG/article/view/141
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